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Statements

Subject Item
n2:RIV%2F61988987%3A17310%2F10%3AA1100YKF%21RIV11-GA0-17310___
rdf:type
n8:Vysledek skos:Concept
dcterms:description
Widened discontinuities (among them crevice-type caves) are characteristic phenomena of landslides in anisotropic rock massifs forming the Flysch Carpathians. We tested the reliability of 2D electrical resistivity tomography (ERT) in the detection of well-mapped cave passages and then tried to explore new subsurface cavities in three sites of crevice-type caves in the Polish Flysch Carpathians. The reliability of ERT detection of potential caves was verified by speleological exploration of a newly discovered cave at the Jaskinia Miecharska site following the ERT campaign. Widened discontinuities (among them crevice-type caves) are characteristic phenomena of landslides in anisotropic rock massifs forming the Flysch Carpathians. We tested the reliability of 2D electrical resistivity tomography (ERT) in the detection of well-mapped cave passages and then tried to explore new subsurface cavities in three sites of crevice-type caves in the Polish Flysch Carpathians. The reliability of ERT detection of potential caves was verified by speleological exploration of a newly discovered cave at the Jaskinia Miecharska site following the ERT campaign.
dcterms:title
Gravitationally induced caves and other discontinuities detected by 2D electrical resistivity tomography: Case studies from the Polish Flysch Carpathians Gravitationally induced caves and other discontinuities detected by 2D electrical resistivity tomography: Case studies from the Polish Flysch Carpathians
skos:prefLabel
Gravitationally induced caves and other discontinuities detected by 2D electrical resistivity tomography: Case studies from the Polish Flysch Carpathians Gravitationally induced caves and other discontinuities detected by 2D electrical resistivity tomography: Case studies from the Polish Flysch Carpathians
skos:notation
RIV/61988987:17310/10:A1100YKF!RIV11-GA0-17310___
n3:aktivita
n15:P
n3:aktivity
P(GAP209/10/0309), P(GP205/06/P185)
n3:cisloPeriodika
1-2
n3:dodaniDat
n5:2011
n3:domaciTvurceVysledku
n4:8228205 n4:4587928 n4:1606530
n3:druhVysledku
n13:J
n3:duvernostUdaju
n17:S
n3:entitaPredkladatele
n18:predkladatel
n3:idSjednocenehoVysledku
261007
n3:idVysledku
RIV/61988987:17310/10:A1100YKF
n3:jazykVysledku
n10:eng
n3:klicovaSlova
2D electrical resistivity tomography; Electrode array; Crevice-type caves; Slope deformations; Mass movements; Polish Flysch Carpathians
n3:klicoveSlovo
n9:Slope%20deformations n9:Crevice-type%20caves n9:2D%20electrical%20resistivity%20tomography n9:Mass%20movements n9:Electrode%20array n9:Polish%20Flysch%20Carpathians
n3:kodStatuVydavatele
NL - Nizozemsko
n3:kontrolniKodProRIV
[E2309FE2160C]
n3:nazevZdroje
GEOMORPHOLOGY
n3:obor
n7:DE
n3:pocetDomacichTvurcuVysledku
3
n3:pocetTvurcuVysledku
6
n3:projekt
n12:GAP209%2F10%2F0309 n12:GP205%2F06%2FP185
n3:rokUplatneniVysledku
n5:2010
n3:svazekPeriodika
123
n3:tvurceVysledku
TÁBOŘÍK, Petr Hradecký, Jan Szura, Czesław Margielewski, Włodzimierz Pánek, Tomáš Urban, Jan
n3:wos
000282732600014
s:issn
0169-555X
s:numberOfPages
15
n16:organizacniJednotka
17310